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ERODED ROCK PILLARS
Eroded rock pillars. These pillars, an example of differential erosion, are a geological feature known as hoodoos. They are formed by wind erosion of loose sandstone, which has formed over harder, more resistant sandstone. Photographed on the banks of the Chilcotin River, in Farwell Canyon, British Columbia, Canada. (KEYSTONE/SCIENCE PHOTO LIBRARY/DAVID NUNUK)
Instruktionen
COPYRIGHTPFLICHTIG
Lizenz
Rights Managed
Erstellungsdatum
20031029
Ort
Credit
KEYSTONE
Source
SCIENCE PHOTO LIBRARY SPL
Byline
DAVID NUNUK
Grösse
7332 x 2385 px
Dateityp
JPEG